The Spanish Coastal Systems 2018
DOI: 10.1007/978-3-319-93169-2_14
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Beaches of Cadiz

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Cited by 5 publications
(5 citation statements)
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“…The bars have a seasonal behavior and their position is influenced by the rocky outcrop [36]. The shoreline position is stable, with long-term erosion rates below 0.75 m/yr [37].…”
Section: Methodology 21 Study Site: Victoria Beachmentioning
confidence: 99%
“…The bars have a seasonal behavior and their position is influenced by the rocky outcrop [36]. The shoreline position is stable, with long-term erosion rates below 0.75 m/yr [37].…”
Section: Methodology 21 Study Site: Victoria Beachmentioning
confidence: 99%
“…On the other hand, even though the easterly winds are more intense and, thus, favorable for dune formation (low moisture content and high speeds), their generating capacity is limited, as they blow almost parallel to the coast. Accordingly, the Camposoto dunes, as well as most of the dunes in the littoral of Cadiz, are formed via westerly winds, which blow perpendicularly and/or obliquely to the coast (Figure 2B; [42]).…”
Section: Study Areamentioning
confidence: 99%
“…Regarding the meteorology, the Guadiaro river is characterized by its irregular and strong dependence on rainfall regime and torrential character [11,53,54], the sand spit behavior being strongly dependent on the river, and by the sea being dependent on E winds and consequent wave behavior [11]. On the other hand, Sotogrande beach suffers from chronical erosion trends, having a regression by more than 160 m which was evident between 1960 and 2000, and is still going (−3.1 m/year) [55]. This implies an increase in vulnerability to climate change due to forecasts of increased wave energy [9][10][11]56].…”
Section: Study Areamentioning
confidence: 99%
“…For the Guadiaro river mouth, the sand spit, and the surrounding beaches, we achieved the following results: (1) regarding the sand spit, especially in 2020 it remained closed throughout the summer season, most likely associated with the COVID-19 pandemic, during which many international tourists were not able to visit Sotogrande, reducing anthropogenic pressure, including urban waste; (2) through climatologies we evaluate how additional small sand bars could be caused by the northward longitudinal current blocked after the construction of Sotogrande harbor; (3) [55] replenishing of beaches can also be detected and monitored by means of S2 images, as demonstrated in the variability of the beach to the south of the Port of Sotogrande in 2017; and (4) the land-sea interface of sandy beaches is more easily identified in different studies throughout the globe compared to rocky beaches or coastal cliffs [36,61,73,74], mostly due to image spatial resolution [75]. However, while S2 undoubtedly enhanced its spatial resolution up to 10 m and, consequently, enhancing the rocky beach delineation, other effects, such as the presence of natural areas of water accumulation on the rocky beach, can lead to misinterpretation, as happened on the Torreguadiaro beach.…”
Section: Contributions To Coastal Managementmentioning
confidence: 99%